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Giant crystals in Mexican cave face dehydration

Water loss from the gypsum crystal surfaces is a primary degradation pathway

by Emma Hiolski, special to C&EN
June 27, 2018


Photo of a geologist standing in the Cave of Crystals (Cueva de los Cristales) in Naica Mine, Chihuahua, Mexico.
Credit: Javier Trueba/MSF/Science Source
In the Cave of Crystals, gypsum crystals have grown up to 12 m long.

In a cave below a mountain in the Naica mine of Chihuahua, Mexico, gypsum crystals have grown as big as trees. But researchers now report that loss of water may damage the crystal surfaces (Cryst. Growth Des. 2018, DOI: 10.1021/acs.cgd.8b00583). By learning more about the gigantic crystals’ degradation, the scientists hope to better preserve them for generations to come.

The crystals—a form of gypsum called selenite (CaSO4∙2H2O)—took up to a million years to develop within a water-filled, magma-heated cave 300 m below the Earth’s surface. By the time the Cave of Crystals was discovered in 2000, nearby mining activity had already drained away the water.

María Elena Montero-Cabrera of the Center for Research in Advanced Materials and her colleagues wanted to learn how the new conditions in the cave might affect the crystals. They put fragments of a large cave crystal under 16 distinct sets of conditions that varied the exposure to four different atmospheres, two different temperatures, and the presence or absence of water.

The team expected that carbon dioxide exposure would cause calcium carbonate to form on the crystal surface, Montero-Cabrera says. However, both infrared spectrometry and grazing incidence X-ray diffraction analysis revealed no detectable calcium carbonate. Instead they found bassanite (CaSO4∙½H2O), a dehydrated form of gypsum crystal. This conversion could, over many years, cloud and scar the crystal surfaces by creating pits and flakes.

The dehydration occurred primarily in environments that did not include water. However, Montero-Cabrera points out that the team designed the degradation scenarios to be harsher than the actual cave environment, so natural crystal dehydration likely occurs at a slower rate.


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